Volatile organic sulfur compounds and their degradation products play important environmental roles in global warming, acid precipitation, and cloud formation. Two important members of this group, dimethyl sulfide, DMS, and methanethiol, MT, are formed by living organisms as well as by abiotic processes. DMS is synthesized by various organisms in the marine environment and large quantities of it are released to the atmosphere. One key precursor for DMS synthesis is the sulfonium salt, dimethylsulfoniopropionate. MT, also formed in marine environments, can be further converted to DMS. The chemical reactions responsible for the biosynthesis of DMS and MT are emphasized here, as well as means for their degradation. Since sulfur compounds are often ignored in normal course work, this article provides a basic foundation for an understanding of these interesting and environmentally significant compounds.
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Chasteen et al. (2004) studied this question.
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